拉武火山 的英文怎麼說

中文拼音 [huǒshān]
拉武火山 英文
gunung lawu
  • : 拉構詞成分。
  • : Ⅰ形容詞1 (關于軍事的) military 2 (關于技擊的) connected with the art of attack and defence in...
  • : fire
  • : 名詞1 (地面形成的高聳的部分) hill; mountain 2 (形狀像山的東西) anything resembling a mountain...
  • 火山 : [地質學] volcano; burning mountain
  1. By studying, the main conclusions have been achieved as follows : i. the volcanic rocks, as the result of the partial melting of enriched mantle, comprise calc - alkaline andesite and dacite and a few tholeiite

    通過研究,得出以下主要認識: 1 、巖為一套以鈣堿性安巖為主,含少量斑玄巖和英安巖。
  2. On the basis of the study on the petrology, trace element, and isotopic geochemistry, the primary magma of volcanic rocks can be divided into two series according to their originated rocks and degree of partial melting. one is the basanite - alkaline basalt - olivine tholeiite magma series, which are generated by partial melting from spinel iherzolite ; the other is nephelinite magma - alkaline picritic basalt magma, which are generated by partial melting of the garnet iherzolite

    巖石化學、微量元素、同位素地球化學證據都表明,華北、華南地區的巖根據源巖和局部熔融程度的不同,可以分為兩個原生巖漿系列:一個是源巖為尖晶石二輝橄欖巖,隨著局部熔融程度的增加,形成的碧玄巖巖漿-堿性玄巖巖漿-橄欖斑玄巖巖漿;另一個是源巖為石榴石二輝橄欖巖,隨著局部熔融程度的增加形成的霞石巖巖漿-堿性苦橄玄巖系列。
  3. From the spatiotemporal distribution of the volcanics of kalagang frn. and tiaohu fm., we can see that there are not only eruptive facies such as rhyolite but also effusion facies such as andesite, basalt and shallow intrusive rock inside the basin

    從三塘湖盆地下二疊統卡崗組及中二疊統條湖組巖的時空分佈特徵可以看出,研究區既發育噴發相的流紋巖,又發育溢流相的玄巖、安巖及淺成侵入巖。
  4. This important tectonic zone parallel to the isotopic geochemical steep zone, which represented a suture line between the yangtze and cathaysian blocks. the geochemical evidence of the jianshui volcanic rocks from the sw part of shizong - mile zone shows that their lithologic types are tholeiites with the comparative flat ree patterns and enrichment in th, depletion slightly in nb, ta, and flat hfse. thus, they may be formed in a back - arc basin with the characteristics between morb and island - a

    該構造帶西南段的建水巖地球化學特徵研究表明,該巖為斑玄巖,具有較平坦的稀土分配型式, th較富集, nb 、 ta輕微虧損,高場強元素分佈較平坦,具有介於島弧和morb之間的地球化學特徵,可能形成於弧后盆地環境。
  5. The lower paleozoic strata in the south kunlun massif are kulafuhe group of cambbrian - ordovician. they consists of metamorphic detrital rocks, limestone, magnetite - bearing basalt, quartzite ( meta - silicalite ), which suggests that they might form at active continent margin. the geochemical characteristics of volcanic and detrital rocks do indicate that they might form at an active marginal environment such as island arc etc. associated with the qimanyuter ophiolite suit, there are lots of early paleozoic granitic plutons

    在昆南地塊上的早古生代地層為寒?奧陶系庫甫河巖群,由變碎屑巖、灰巖、含磁鐵礦玄巖、石英巖(變硅質巖)等組成,顯示其比昆北地塊有較大的活動性,巖和碎屑巖的巖石地球化學特徵也反映為島弧及活動邊緣環境。
  6. He ' s run arms to rebel forces in rwanda, sierra leone, angola,

    他給盧安達、獅子、安哥的反政府裝提供軍發戰爭財
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